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    Near-Inertial Oscillations of a Barotropic Vortex: Trapped Modes and Time Evolution 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 004:;page 747
    Author(s): Llewellyn Smith, Stefan G.
    Publisher: American Meteorological Society
    Abstract: Amplified motions in vortices have been observed in Gulf Stream rings and over seamounts. This paper uses the near-inertial oscillation approximation to model near-inertial motions in the presence of a barotropic vortical ...
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    Hydraulically Drained Flows in Rotating Basins. Part I: Method 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 012:;page 2509
    Author(s): Pratt, Lawrence J.; Llewellyn Smith, Stefan G.
    Publisher: American Meteorological Society
    Abstract: An asymptotic method for coupling circulations in basins to hydraulically controlled overflows is introduced. The method is applicable when the forcing, dissipation, and coupling with the overflow are weak, in which case ...
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    Radiation of Mixed Layer Near-Inertial Oscillations into the Ocean Interior 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 006:;page 1550
    Author(s): Moehlis, J.; Llewellyn Smith, Stefan G.
    Publisher: American Meteorological Society
    Abstract: The radiation from the mixed layer into the interior of the ocean of near-inertial oscillations in the presence of the beta effect is reconsidered as an initial-value problem. Making use of the fact that the mixed layer ...
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    Conversion of the Barotropic Tide 

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 005:;page 1554
    Author(s): Llewellyn Smith, Stefan G.; Young, W. R.
    Publisher: American Meteorological Society
    Abstract: Using linear wave theory, the rate at which energy is converted into internal gravity waves by the interaction of the barotropic tide with topography in an ocean is calculated. Bell's formula for the conversion rate is ...
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    Velocity Probability Density Functions from Altimetry 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 001:;page 125
    Author(s): Gille, Sarah T.; Llewellyn Smith, Stefan G.
    Publisher: American Meteorological Society
    Abstract: Probability density functions (pdfs) are employed to evaluate the distribution of velocities in the global ocean. This study computes pdfs of ocean surface velocity using altimetric data from the TOPEX/Poseidon satellite. ...
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    Energy Cascades and Loss of Balance in a Reentrant Channel Forced by Wind Stress and Buoyancy Fluxes 

    Source: Journal of Physical Oceanography:;2014:;Volume( 045 ):;issue: 001:;page 272
    Author(s): Barkan, Roy; Winters, Kraig B.; Llewellyn Smith, Stefan G.
    Publisher: American Meteorological Society
    Abstract: large fraction of the kinetic energy in the ocean is stored in the ?quasigeostrophic? eddy field. This ?balanced? eddy field is expected, according to geostrophic turbulence theory, to transfer energy to larger scales. In ...
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    The Propagation of Tsunami-Generated Acoustic–Gravity Waves in the Atmosphere 

    Source: Journal of the Atmospheric Sciences:;2016:;Volume( 073 ):;issue: 008:;page 3025
    Author(s): Wu, Yue; Llewellyn Smith, Stefan G.; Rottman, James W.; Broutman, Dave; Minster, Jean-Bernard H.
    Publisher: American Meteorological Society
    Abstract: sunami-generated acoustic?gravity waves have been observed to propagate in the atmosphere up to the ionosphere, where they have an impact on the total electron content. The authors simulate numerically the propagation of ...
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    Bifurcation of a Coastal Current at an Escarpment 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 005:;page 969
    Author(s): Carnevale, George F.; Llewellyn Smith, Stefan G.; Crisciani, Fulvio; Purini, Roberto; Serravall, Roberta
    Publisher: American Meteorological Society
    Abstract: The evolution of a coastal current as it encounters an escarpment depends strongly on whether the geometry of the coast and escarpment is right or left ?handed,? independent of the direction of the coastal current. Handedness ...
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